Nurpeisova  M.B., Kurgizbaeva G.M., Tursbekov S.V.

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METHODS OF STUDIES OF DANGEROUS TECTONIC PROCESSES

 

      Efficacy and safety of works while there are mining operations and the commissioning of facilities that fall into the affected zone of these actions, depend on the geodynamic state of the strata and tectonic and anthropogenic processes occurring in it. Meanwhile, the design of mining enterprises are generally implemented on the basis of very little information about the state of rock mass, because direct observations at the site of the future object prior to mining is simply impossible.  These problems and difficulties are eliminated with geodynamic monitoring. The main objective of the monitoring is to provide timely information about geo-mechanical processes in the strata and surface and their consequences. This information is necessary for taking timely preventive measures.

     In accordance with the Regulations on the geological and surveying of industrial safety and protection of resources in the Law on Subsoil and Subsoil Use No 2828, Law on natural and anthropogenic emergency situations, the Regulations on State monitoring of subsoil of Republic of Kazakhstan, surveying services keep monitoring subsoil. This includes the processes of rock and earth surface movement, geo-mechanical and geodynamic processes while subsoil use in order to prevent harmful effects of mining on capital mining, objects of the earth surface and environment.

      Figure 1 shows the projected structure of methods of study and forecast of dangerous states in the natural-technical system, taking into account the full range of geophysical and geodetic measurements and their joint processing.

On the basis of the analysis of geology and tectonics of the area, numerical modeling and experimental assessments of the stress state in the mass “energy-zones” are allocated; they define the boundaries of the geodynamic monitoring zones. Then the monitoring of the danger zone is organized which includes mainly control of the deformation and the parameters of geophysical fields.

Reliable information on the deformations of rock mass can be obtained by direct geodetic observations on the geodynamic grounds. Earth surface shifting (ESS) are studied by the method of re-leveling according to the first class method, when measurements are analyzed exceeding by sections between adjacent benchmarks. Leveling technology should comply with accepted methodology.

The principle of leveling is based on the processing of the encoded signal (obtained from the slat through the lens). The microprocessor calculates the reading of the slat and the corresponding horizontal distance between the slat and level. The measurement results are stored in the REK of WILD GRM 10 module with the subsequent transfer of data into the computer and data processing with the special program. The advantage of this system is the simplicity of measurement, trueness of readout and writing, automatic calculation of heights during the measurement and recording of data.

 

 

 


      

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 


Figure 2 - Scheme of methods of study and prediction of geodynamic phenomena in the NTS

 

With increasing accuracy and efficiency of geodetic measurements the range of problems is expanded. Modern geodesy can make a significant contribution to their solutions. One of these problems is the detailed study of anthropogenic processes. Its decision would create permanent operating geodynamic anthropogenic grounds, based on regularly performed geophysical and geodetic observations with the interpretation of their results from the viewpoint of geodesy.

High-precision geodetic observations are conducted on the geodynamic grounds by the surveying services. The increased volumes and intensity of mineral resources development produce the beginning of anthropogenic disasters that are associated with certain shifts and subsidence of earth surface.

Technology of satellite system (GPS - Technology) turned out to be very effective among the modern methods and tools for the study of displacements and deformations of the earth surface. Satellite systems GPS (Global Positioning System) are necessary for creation a basis for the calculation of deformation and geographic information systems that allow predicting the parameters of geodynamic processes. Along with the GPS-technology systematic observation are conducted of ESS with tachometers and digital levels for different areas of intensive mining of solid minerals.

 

Literature:

1. Nurpeisova M.B., Kyrgizbayeva G.M.: Guidelines for monitoring pitedges deformations and assessing sustainability. -Almaty, KazNTU, 2003.-33p.

2. Nurpeisova M.B., Bekbasarov Sh.Sh. Environmental problems of mineral resources development. - Almaty, 2006, Journal of KazNTU .- P.3-5